Magnitude Scales for Marsquakes

被引:18
作者
Boese, Maren [1 ]
Giardini, Domenico [1 ]
Staehler, Simon [1 ]
Ceylan, Savas [1 ]
Clinton, John Francis [2 ]
van Driel, Martin [1 ]
Khan, Amir [1 ]
Euchner, Fabian [2 ]
Lognonne, Philippe [3 ]
Banerdt, William Bruce [4 ]
机构
[1] Swiss Fed Inst Technol, Inst Geophys, Sonneggstr 5, CH-8092 Zurich, Switzerland
[2] Swiss Fed Inst Technol, Swiss Seismol Serv SED, Sonneggstr 5, CH-8092 Zurich, Switzerland
[3] Univ Paris Diderot, Inst Phys Globe Paris, 35 Rue Helene Brion, F-75205 Paris, France
[4] CALTECH, Jet Prop Lab, M-S 321-B60,4800 Oak Grove Dr, Pasadena, CA 91109 USA
基金
瑞士国家科学基金会;
关键词
INSIGHT MISSION; SINGLE-STATION; BULK COMPOSITION; MARS SEISMICITY; ENERGY-RELEASE; SEISMOGRAMS; EARTH; LOCATION; MODELS; NOISE;
D O I
10.1785/0120180037
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In anticipation of the upcoming 2018 InSight (Interior exploration using Seismic Investigations, Geodesy and Heat Transport) Discovery mission to Mars, we calibrate magnitude scales for marsquakes that incorporate state-of-the-art knowledge on Mars interior structure and the expected ambient and instrumental noise. We regress magnitude determinations of 2600 randomly distributed marsquakes, simulated with a spectral element method for 13 published 1D structural models of Mars' interior. The continuous seismic data from InSight will be returned at 2 samples per second. To account for this limited bandwidth as well as for the expected noise conditions on Mars, we define and calibrate six magnitude scales: (1) local Mars magnitude M-L(Ma) at a period of 3 s for marsquakes at distances of up to 10 degrees; (2) P-wave magnitude m(b)(Ma); (3) S-wave magnitude m(bS)(Ma) each defined at a period of 3 s and calibrated for distances from 5 degrees to 100 degrees; (4) surface-wave magnitude M-s(Ma) defined at a period of 20 s, as well as (5) moment magnitudes M-FB(Ma); and (6) M-F(Ma) computed from the low-frequency (10-100 s) plateau of the displacement spectrum for either body waves or body and surface waves, respectively; we calibrate scales (4)-(6) for distances from 5 degrees to 180 degrees. We regress stable calibrations of the six scales with respect to the seismic moment magnitude at M-w 5.5 by correcting filtered phase amplitudes for attenuation with distance and source depth. Expected errors in epicentral distance and in source depth (25% and 20 km, respectively) translate into magnitude errors of 0.1-0.3 units. We validate our magnitude relations with an independent test dataset of 2600 synthetic marsquakes (1.0 <= M-w <= 7.0), for which seismograms are superimposed on the realistic noise predicted by the InSight noise model. Marsquakes with M-w < 3.0 and epicentral distances of Delta > 15 degrees are expected to be hidden in the Mars background noise and will likely not be detectable.
引用
收藏
页码:2764 / 2777
页数:14
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